词条 | Great Salinity Anomaly |
释义 |
The Great Salinity Anomaly originally referred to a significant disturbance caused by a major pulse of freshwater input to the Nordic Seas in the late 1960s and early 1970s.[1](Hakkinen. 1999) Since the discovery of this GSA, the term "Great Salinity Anomaly" has been applied to successive occurrences of the same phenomenon, including the Great Salinity Anomaly of the 1980s[2] and the Great Salinity Anomaly of the 1990s.[3] The recovery time for reversion of such anomalies is typically on the order of several years. (Belkin. 2004) A Great Salinity Anomaly affects sea basins over a wide geographical distance, as seawater moved from one basin to another; this propagation affected numerous far northern sea basins, with the latest arrival being the Norwegian Sea. (Hogan. 2011) ResearchRecent studies (2017) suggest potential subpolar North Atlantic (SPG) convection collapse, resulting in rapid North Atlantic cooling, and assess AMOC slow or shutdown.[4] References1. ^{{cite web|url= http://www.mindfully.org/Water/2005/Fresh-Water-N-Atlantic16jun05.htm html|title= How Much Excess Fresh Water Was Added to the North Atlantic in Recent Decades? }} 2. ^{{cite journal|url= http://www.sciencedirect.com/science/article/pii/S0079661198000159|title= "Great Salinity Anomalies" in the North Atlantic | doi=10.1016/S0079-6611(98)00015-9 | bibcode=1998PrOce..41....1B|volume=41|journal=Progress in Oceanography|pages=1–68|author=Belkin Igor M}} 3. ^{{cite web|url= http://www.agu.org/pubs/crossref/2004/2003GL019334.shtml|title= Propagation of the "Great Salinity Anomaly" of the 1990s around the northern North Atlantic}} 4. ^{{cite web|title=Abrupt cooling over the North Atlantic in modern climate models|doi=10.1038/ncomms14375|url=https://www.nature.com/articles/ncomms14375|author=Sgubin|display-authors=etal|year=2017|publisher=Nature}}
1 : Oceanography |
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